The U. S. Geological Survey and the Ohio Division of Water conducted a refraction seismic survey of the Little Miami River valley near Xenia, Ohio, and the Scioto River valley between Columbus and Chillicothe, Ohio, in the fall of 1963.
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Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha80","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"80","title":"Water-table, surface-drainage, and engineering soils map of the Taylors bridge area, Delaware","language":"ENGLISH","doi":"10.3133/ha80","usgsCitation":"Adams, J.K., and Boggess, D.H., 1964, Water-table, surface-drainage, and engineering soils map of the Taylors bridge area, Delaware: U.S. Geological Survey Hydrologic Atlas 80, col. map ;on sheet 74 x 92 cm., https://doi.org/10.3133/ha80.","productDescription":"col. map ;on sheet 74 x 92 cm.","costCenters":[],"links":[{"id":185698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90289,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/080/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.61749999999999,39.3675 ], [ -75.61749999999999,39.5 ], [ -75.5,39.5 ], [ -75.5,39.3675 ], [ -75.61749999999999,39.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c90","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":976,"text":"wsp1669CC - 1964 - Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","interactions":[{"subject":{"id":976,"text":"wsp1669CC - 1964 - Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","indexId":"wsp1669CC","publicationYear":"1964","noYear":false,"chapter":"CC","title":"Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins"},"predicate":"IS_PART_OF","object":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"id":1}],"isPartOf":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"lastModifiedDate":"2023-01-06T19:58:08.762707","indexId":"wsp1669CC","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1669","chapter":"CC","title":"Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","docAbstract":"The average daily load of the Brazos River at Possum Kingdom Reservoir is about 2,800 tons of dissolved solids, of which 1,000 tons is chloride. More than 85 percent of the chloride load is contributed by the Salt Fork Brazos River, and more than 50 percent of the chloride load of the Brazos River originates from salt springs and seeps in Croton and Salt Crotdn Creeks, which are tributaries of Salt Fork Brazos River. The rest of the chloride is contributed from many small sources.
\nThe average daily chloride load of Croton Creek is 70 tons, much of which is carried during periods of flood runoff. The average daily chloride load of Salt Croton Creek is about 480 tons. Of this total, 330 tons is contributed by the base flow, which ranges from 0.5 to 2 cubic feet per second.
\nThe principal areas of salt springs and seeps in the Croton Creek basin are Hot Springs and Short Croton Salt Flats in northeastern Kent County. In the Salt Croton Creek basin, saline water is discharged in Dove Creek Salt Flat, Dove Creek near Dove Creek Salt Flat, and three small salt flats on Haystack Creek, all in southwestern King County and northwestern Stonewall County.
\nSalt springs and seeps discharge from the rocks of the Whitehorse Group undifferentiated in the Croton Creek basin, and from the upper part of the Dog Creek Shale of the Pease River Group in the Salt Croton Creek basin. Both groups are of Permian age. The water that is discharged by springs and seeps in the Croton Creek basin is derived from the infiltration of precipitation and seepage from streams in the Duck Creek basin. The source of the water that discharges in the Salt Croton basin is not known.
\nThe salt load contributed to the Brazos River by the springs and seeps can be reduced, although the volume of salt water for disposal probably cannot be reduced or eliminated. Collecting and disposing of the base flow of Salt Croton Creek would reduce the salt load of the Brazos River by 30 percent; disposal of the total flow of Salt Croton Creek would reduce the salt load by 45 percent.
\nThe salt water may be disposed of by impounding it in reservoirs for evaporation or by injecting it underground through oil wells, oil tests, or wells drilled for saltwater disposal. Sediments in which the salt water possibly could be injected underlie the. Dove Creek Salt Flats at depths of less than 7,000 feet.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962 (Water Supply Paper 1669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1669CC","usgsCitation":"Baker, R.C., Hughes, L.S., and Yost, I.D., 1964, Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins: U.S. Geological Survey Water Supply Paper 1669, Report: vi, 81 p. ; 4 Plates: 36.00 x 35.86 inches or smaller, https://doi.org/10.3133/wsp1669CC.","productDescription":"Report: vi, 81 p. ; 4 Plates: 36.00 x 35.86 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":411514,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24863.htm","linkFileType":{"id":5,"text":"html"}},{"id":25542,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669cc/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25538,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25539,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669cc/report-thumb.jpg"},{"id":25540,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25541,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Brazos River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -100.25,\n 33.25\n ],\n [\n -100.25,\n 32.5\n ],\n [\n -98.75,\n 32.5\n ],\n [\n -98.75,\n 33.25\n ],\n [\n -100.25,\n 33.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980df","contributors":{"authors":[{"text":"Baker, R. C.","contributorId":79084,"corporation":false,"usgs":true,"family":"Baker","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":142954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, Leon S.","contributorId":65056,"corporation":false,"usgs":true,"family":"Hughes","given":"Leon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":142953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yost, I. D.","contributorId":12833,"corporation":false,"usgs":true,"family":"Yost","given":"I.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":142952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26,"text":"wsp1727 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 4. St. Lawrence River basin","interactions":[],"lastModifiedDate":"2022-01-31T12:17:02.543877","indexId":"wsp1727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1727","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 4. St. Lawrence River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1727","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 4. St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1727, Report: x, 379 p.; 1 Plate: 40.50 x 24.06 inches, https://doi.org/10.3133/wsp1727.","productDescription":"Report: x, 379 p.; 1 Plate: 40.50 x 24.06 inches","costCenters":[],"links":[{"id":24641,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1727/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24642,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1727/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395101,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24911.htm"},{"id":136419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1727/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Michigan, Minnesota, New York, Pennsylvania, Wisconsin","otherGeospatial":"St. Lawrence River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.98828125,\n 40.697299008636755\n ],\n [\n -73.828125,\n 40.697299008636755\n ],\n [\n -73.828125,\n 47.945786463687185\n ],\n [\n -92.98828125,\n 47.945786463687185\n ],\n [\n -92.98828125,\n 40.697299008636755\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9860","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25,"text":"wsp1726 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 3–B. Cumberland and Tennessee River Basins","interactions":[],"lastModifiedDate":"2022-01-28T22:04:28.312267","indexId":"wsp1726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1726","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 3–B. Cumberland and Tennessee River Basins","docAbstract":"No abstract available.
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Cumberland and Tennessee River Basins: U.S. Geological Survey Water Supply Paper 1726, Report: viii, 269 p.; 1 Plate: 28.00 × 19.74 inches, https://doi.org/10.3133/wsp1726.","productDescription":"Report: viii, 269 p.; 1 Plate: 28.00 × 19.74 inches","costCenters":[],"links":[{"id":24639,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1726/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1726/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395100,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24910.htm"},{"id":136418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1726/report-thumb.jpg"}],"country":"United States","state":"Kentucky, North Carolina, Tennessee","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.27490234375,\n 35.11990857099681\n ],\n [\n -82.4853515625,\n 35.11990857099681\n ],\n [\n -82.4853515625,\n 38.324420427006544\n ],\n [\n -89.27490234375,\n 38.324420427006544\n ],\n [\n -89.27490234375,\n 35.11990857099681\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9836","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527156,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32704,"text":"pp474F - 1964 - Water content of micas and chlorites","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"pp474F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"474","chapter":"F","title":"Water content of micas and chlorites","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1963","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp474F","usgsCitation":"Foster, M., 1964, Water content of micas and chlorites: U.S. Geological Survey Professional Paper 474, p. F1-F15, https://doi.org/10.3133/pp474F.","productDescription":"p. F1-F15","costCenters":[],"links":[{"id":119139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0474f/report-thumb.jpg"},{"id":60596,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0474f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0474f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa23b","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":97958,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret D.","affiliations":[],"preferred":false,"id":208978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":972,"text":"wsp1694 - 1964 - Geology and ground-water conditions in the Wilmington-Reading area, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1694","title":"Geology and ground-water conditions in the Wilmington-Reading area, Massachusetts","docAbstract":"The Wilmington-Reading area, as defined for this report, contains the headwaters of the Ipswich River in northeastern Massachusetts. Since World War II the growth of communities in this area and the change in character of some of them from rural to suburban have created new water problems and intensified old ones. The purpose of this report on ground-water conditions is to provide information that will aid in understanding and resolving some of these problems. \r\n\r\nThe regional climate, which is humid and temperate, assures the area an ample natural supply of water. At the current stage of water-resources development a large surplus of water drains from the area by way of the Ipswich River during late autumn, winter, and spring each year and is unavailable for use during summer and early autumn, when during some years there is a general water deficiency. \r\n\r\nGround water occurs both in bedrock and in the overlying deposits of glacial drift. The bedrock is a source of small but generally reliable supplies of water throughout the area. Glacial till also is a source of small supplies of water, but wells in till often fail to meet modern demands. Stratified glacial drift, including ice-contact deposits and outwash, yields small to large supplies of water. \r\n\r\nStratified glacial drift forms the principal ground-water reservoir. It partly fills a system of preglacial valleys corresponding roughly to the valleys of the present Ipswich River system and is more than 100 feet thick at places. The ice-contact deposits generally are more permeable than the outwash deposits. Ground water occurs basically under water-table conditions. \r\n\r\nRecharge in the Wilmington-Reading area is derived principally from precipitation on outcrop areas of ice-contact deposits and outwash during late autumn, winter. and spring. It is estimated that the net annual recharge averages about 10 inches and generally ranges from 5 inches during unusually dry years to 15 inches during unusually wet years. Ground water withdrawn largely by municipal wells supplies the towns of North Reading, Reading, and Wilmington. In 1957 the average daily withdrawal from these wells was about 2.5 million gallons, of which about half was used outside the Ipswich River drainage basin. \r\n\r\nThe chemical quality of the ground water is generally satisfactory except for local excessive concentrations of iron. \r\n\r\nThe storage capacity of the ground-water reservoir and recharge in the Wilmington-Reading area are large enough to sustain a total withdrawal of ground water at several times the current rate, but the use of the reservoir probably will be limited by the extent to which wells of moderate or large capacity can be dispersed. This will depend upon the distribution of areas of thick permeable materials. Conditions in the Martins Brook-Skug River drainage basin seem generally favorable for increased development of water supplies. In the rest of the Wilmington-Reading area the chances of finding substantial bodies of thick permeable materials probably are small, but further exploration is desirable. \r\n\r\nMeasures proposed to drain swampland by deepening and straightening the Ipswich River and its tributaries will have some effect upon the ground-water conditions. Probably the most obvious effect will be a lowering of water levels in wells near improved reaches of channel. Also important will b the effect of changes in low streamflow conditions on wells that induce infiltration from streams and the effect on well yields of an improved hydraulic connection between streams and the ground-water body. \r\n\r\nThe Reading 100-acre well field, which derives part of its supply by inducing recharge from the Ipswich River, would be affected by the drainage measures. During a dry summer, such as that of 1957, the flow of the Ipswich is fully diverted by pumping at this well field, and drawdowns at some of the wells approach half the saturated thickness of the aquifer there. If the drainage measures are","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1694","usgsCitation":"Baker, J.A., Healy, H., and Hackett, O.M., 1964, Geology and ground-water conditions in the Wilmington-Reading area, Massachusetts: U.S. Geological Survey Water Supply Paper 1694, v, 80 p. :ill., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1694.","productDescription":"v, 80 p. :ill., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":137045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1694/report-thumb.jpg"},{"id":25518,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1694/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25519,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1694/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25520,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1694/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25521,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1694/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25522,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1694/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6860c9","contributors":{"authors":[{"text":"Baker, John Augustus","contributorId":48159,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"Augustus","affiliations":[],"preferred":false,"id":142946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, H.G.","contributorId":72776,"corporation":false,"usgs":true,"family":"Healy","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":142947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":142945,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32778,"text":"pp440L - 1964 - Phase-equilibrium relations of the common rock-forming oxides except water","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"pp440L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"440","chapter":"L","title":"Phase-equilibrium relations of the common rock-forming oxides except water","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Data of geochemistry","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp440L","usgsCitation":"Morey, G., 1964, Phase-equilibrium relations of the common rock-forming oxides except water: U.S. Geological Survey Professional Paper 440, p. 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L1-L159","costCenters":[],"links":[{"id":119279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0440l/report-thumb.jpg"},{"id":60721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0440l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db68792d","contributors":{"authors":[{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":209142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68272,"text":"ha131 - 1964 - Availability of ground water in Hall County, Nebraska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"131","title":"Availability of ground water in Hall County, Nebraska","language":"ENGLISH","doi":"10.3133/ha131","usgsCitation":"Keech, C.F., and Dreeszen, V., 1964, Availability of ground water in Hall County, Nebraska: U.S. Geological Survey Hydrologic Atlas 131, 4 maps ;31 x 29 cm., on sheet 122 x 105 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha131.","productDescription":"4 maps ;31 x 29 cm., on sheet 122 x 105 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":188556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89678,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66724c","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":277947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreeszen, V. H.","contributorId":8825,"corporation":false,"usgs":true,"family":"Dreeszen","given":"V. H.","affiliations":[],"preferred":false,"id":277946,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":974,"text":"wsp1669Y - 1964 - Ground-water resources of the Lowell area, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669Y","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1669","chapter":"Y","title":"Ground-water resources of the Lowell area, Massachusetts","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669Y","usgsCitation":"Baker, J.A., 1964, Ground-water resources of the Lowell area, Massachusetts: U.S. Geological Survey Water Supply Paper 1669, iv, 37 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1669Y.","productDescription":"iv, 37 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669y/report-thumb.jpg"},{"id":25528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669y/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25529,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669y/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25530,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669y/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669y/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db65848f","contributors":{"authors":[{"text":"Baker, John Augustus","contributorId":48159,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"Augustus","affiliations":[],"preferred":false,"id":142949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":986,"text":"wsp1535H - 1964 - Field measurement of alkalinity and pH","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1535H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1535","chapter":"H","title":"Field measurement of alkalinity and pH","docAbstract":"The behavior of electrometric pH equipment under field conditions departs from the behavior predicted from Nernst's law. The response is a linear function of pH, and hence measured pH values may be corrected to true pH if the instrument is calibrated with two reference solutions for each measurement. Alkalinity titrations may also be made in terms of true pH. Standard methods, such as colorimetric titrations, were rejected as unreliable or too cumbersome for rapid field use. The true pH of the end point of the alkalinity titration as a function of temperature, ionic strength, and total alkalinity has been calculated. Total alkalinity in potable waters is the most important factor influencing the end point pH, which varies from 5.38 (0 ? C, 5 ppm (parts per million) HC0a-) to 4.32 (300 ppm HC0a-,35 ? C), for the ranges of variables considered. With proper precautions, the pH may be determined to =i:0.02 pH and the alkalinity to =i:0.6 ppm HCO3- for many naturally occurring bodies of fresh water.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1535H","usgsCitation":"Barnes, I., 1964, Field measurement of alkalinity and pH: U.S. Geological Survey Water Supply Paper 1535, 17 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1535H.","productDescription":"17 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535h/report-thumb.jpg"},{"id":25556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4a3c","contributors":{"authors":[{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":142969,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1278,"text":"wsp1576E - 1964 - Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1576E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1576","chapter":"E","title":"Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico","docAbstract":"The need for additional water has increased in recent years on the Acoma and Laguna Indian Reservations in west-central New Mexico because the population and per capita use of water have increased; the tribes also desire water for light industry, for more modern schools, and to increase their irrigation program. Many wells have been drilled in the area, but most have been disappointing because of small yields and poor chemical quality of the water. \r\n\r\nThe topography in the Acoma and Laguna Indian Reservations is controlled primarily by the regional and local dip of alternating beds of sandstone and shale and by the igneous complex of Mount Taylor. The entrenched alluvial valley along the Rio San Jose, which traverses the area, ranges in width from about 0.4 mile to about 2 miles. \r\n\r\nThe climate is characterized by scant rainfall, which occurs mainly in summer, low relative humidity, and large daily fluctuations of temperature. Most of the surface water enters the area through the Rio San Jose. The average annual streamflow past the gaging station Rio San Jose near Grants, N. Mex. is about 4,000 acre-feet. Tributaries to the Rio San Jose within the area probably contribute about 1,000 acre-feet per year. At the present time, most of the surface water is used for irrigation. \r\n\r\nGround water is obtained from consolidated sedimentary rocks that range in age from Triassic to Cretaceous, and from unconsolidated alluvium of Quaternary age. The principal aquifers are the Dakota Sandstone, the Tres Hermanos Sandstone Member of the Mancos Shale, and the alluvium. The Dakota Sandstone yields 5 to 50 gpm (gallons per minute) of water to domestic and stock wells. The Tres Hermanos sandstone Member generally yields 5 to 20 gpm of water to domestic and stock wells. Locally, beds of sandstone in the Chinle and Morrison Formations, the Entrada Sandstone, and the Bluff Sandstone also yield small supplies of water to domestic and stock wells. The alluvium yields from 2 gpm to as much as 150 gpm of water to domestic and stock wells. Thirteen test wells were drilled in a search for usable supplies of ground water for pueblo and irrigation supply and to determine the geologic and hydrologic characteristics of the water-bearing material. The performance of six of the test wells suggests that the sites are favorable for pueblo or irrigation supply wells. The yield of the other seven wells was too small or the quality of the water was too poor for development of pueblo or irrigation supply to be feasible. However, the water from one of the seven wells was good in chemical quality, and the yield was large enough to supply a few homes with water. \r\n\r\nThe tests suggest that the water in the alluvium of the Rio San Jose valley is closely related to the streamflow and that it might be possible to withdraw from the alluvium in summer and replenish it in winter. The surface flow in summer might be decreased by extensive pumpage of ground water, but on the other hand, more of the winter flow could be retained in the area by storage in the ground-water reservoir. Wells could be drilled along the axis of the valley, and the water could be pumped into systems for distribution to irrigated farms. The chemical quality of ground water in the area varies widely from one stratigraphic unit to another and laterally within each unit and commonly the water contains undesirably large amounts of sulfate. However, potable water has been obtained locally from all the aquifers. The water of best quality seemingly is in the Tres Hermanos Sandstone Member of the Mancos Shale and in the alluvium north of the Rio San Jose. The largest quantity of water that is suitable for irrigation is in the valley fill along the Rio San Jose. \r\n\r\nIntensive pumping of ground water from aquifers containing water of good quality may draw water of inferior chemical quality into the wells.","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1576E","usgsCitation":"Dinwiddie, G.A., and Motts, W.S., 1964, Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico: U.S. Geological Survey Water Supply Paper 1576, iv, 65 p. :ill., map ;24 cm. & 3 maps in pocket., https://doi.org/10.3133/wsp1576E.","productDescription":"iv, 65 p. :ill., map ;24 cm. & 3 maps in pocket.","costCenters":[],"links":[{"id":137528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1576e/report-thumb.jpg"},{"id":26238,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26239,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26240,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1576e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db99","contributors":{"authors":[{"text":"Dinwiddie, George A.","contributorId":21135,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motts, Ward Sundt","contributorId":68708,"corporation":false,"usgs":true,"family":"Motts","given":"Ward","email":"","middleInitial":"Sundt","affiliations":[],"preferred":false,"id":143489,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21,"text":"wsp1736 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, Part 12. Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2023-10-30T20:25:05.016716","indexId":"wsp1736","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1736","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, Part 12. Pacific slope basins in Washington and upper Columbia River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1736","usgsCitation":"Hendricks, E.L., Stermitz, F., Travis, W.I., and Veatch, F.M., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, Part 12. Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Water Supply Paper 1736, Report: xii, 415 p.; 1 Plate: 38.00 x 32.00 inches, https://doi.org/10.3133/wsp1736.","productDescription":"Report: xii, 415 p.; 1 Plate: 38.00 x 32.00 inches","costCenters":[],"links":[{"id":422260,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24920.htm","linkFileType":{"id":5,"text":"html"}},{"id":24632,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1736/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24631,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1736/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1736/report-thumb.jpg"}],"country":"Canada, United States","state":"British Columbia, Idaho, Montana, Washington","otherGeospatial":"Columbia River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.83285623417206,\n 46.21526742606159\n ],\n [\n -122.9103575794982,\n 46.10019062260318\n ],\n [\n -122.33577550877052,\n 45.546433837088074\n ],\n [\n -120.79326529488043,\n 45.69065022745636\n ],\n [\n -119.01771001579024,\n 45.911112652187285\n ],\n [\n -116.5766946569901,\n 46.57952007425328\n ],\n [\n -112.79118890228793,\n 45.229762147449804\n ],\n [\n -111.56531872612507,\n 44.72217816015629\n ],\n [\n -109.44982072003845,\n 45.31370500822021\n ],\n [\n -109.38824886913031,\n 46.63351149333437\n ],\n [\n -114.58488333343809,\n 49.336191823935536\n ],\n [\n -117.06711312884372,\n 51.706457503061046\n ],\n [\n -119.68391483154326,\n 52.265893001133264\n ],\n [\n -120.8034366801796,\n 49.355099498605085\n ],\n [\n -122.05761659488559,\n 48.98867586437896\n ],\n [\n -123.06668050826144,\n 48.98126333744935\n ],\n [\n -122.8331235873379,\n 48.28878711013357\n ],\n [\n -124.82963267871801,\n 48.47285068332545\n ],\n [\n -124.69085888576103,\n 47.836074310656414\n ],\n [\n -123.83285623417206,\n 46.21526742606159\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9897","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stermitz, Frank","contributorId":15175,"corporation":false,"usgs":true,"family":"Stermitz","given":"Frank","email":"","affiliations":[],"preferred":false,"id":887160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Travis, W. I.","contributorId":47445,"corporation":false,"usgs":true,"family":"Travis","given":"W.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":887161,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Veatch, F. M.","contributorId":97484,"corporation":false,"usgs":true,"family":"Veatch","given":"F.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":887162,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20,"text":"wsp1722 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 1–B. North Atlantic Slope Basins, New York to York River","interactions":[],"lastModifiedDate":"2022-01-28T21:47:58.436514","indexId":"wsp1722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1722","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 1–B. North Atlantic Slope Basins, New York to York River","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1722","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 1–B. North Atlantic Slope Basins, New York to York River: U.S. Geological Survey Water Supply Paper 1722, Report: xiii, 578 p.; 1 Plate: 29.50 × 38.24 inches, https://doi.org/10.3133/wsp1722.","productDescription":"Report: xiii, 578 p.; 1 Plate: 29.50 × 38.24 inches","costCenters":[],"links":[{"id":137533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1722/report-thumb.jpg"},{"id":395098,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24906.htm"},{"id":24630,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1722/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24629,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1722/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut, Delaware, Maryland, Massachusetts, New Jersey, New York, Pennsylvania, Vermont, Virginia, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.9697265625,\n 37.3002752813443\n ],\n [\n -72.5537109375,\n 37.3002752813443\n ],\n [\n -72.5537109375,\n 44.19795903948531\n ],\n [\n -78.9697265625,\n 44.19795903948531\n ],\n [\n -78.9697265625,\n 37.3002752813443\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9934","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32795,"text":"pp372B - 1964 - General effects of drought on water resources of the southwest","interactions":[],"lastModifiedDate":"2022-02-16T22:32:18.53445","indexId":"pp372B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"372","chapter":"B","title":"General effects of drought on water resources of the southwest","docAbstract":"The effects of drought are most pronounced on soil moisture, because soil is the prime recipient of the water from precipitation, and upon streamflow, because it is the residual water that is not accepted by or that flows out from the soil and groundwater reservoirs. Studies by statistical correlation of records of natural streamflow and of dendrochronology indicate patterns of regional runoff that reflect precipitation trends in the principal meteorologic regions in the Southwest. By contrast, the effects of drought upon ground water vary with the natural characteristics and degree of utilization of individual aquifers.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Drought in the Southwest, 1942-56 (Professional Paper 372)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp372B","usgsCitation":"Gatewood, J.S., Wilson, A., Thomas, H.E., and Kister, L., 1964, General effects of drought on water resources of the southwest: U.S. Geological Survey Professional Paper 372, Report: iii, 55 p.; 1 Plate: 16.99 x 20.10 inches, https://doi.org/10.3133/pp372B.","productDescription":"Report: iii, 55 p.; 1 Plate: 16.99 x 20.10 inches","numberOfPages":"59","costCenters":[],"links":[{"id":336002,"rank":7,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372D","text":"Chapter D: Effects of drought in the Rio Grande basin"},{"id":336000,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372A","text":"Chapter A: The meteorologic phenomenon of drought in the Southwest"},{"id":336001,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372C","text":"Chapter C: Effects of drought in central and south Texas"},{"id":336003,"rank":8,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372E","text":"Chapter E: Effects of drought in basins of interior drainage"},{"id":336004,"rank":9,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372F","text":"Chapter F: Effects of drought in the Colorado River basin"},{"id":336005,"rank":10,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372G","text":"Chapter G: Effects of drought along Pacific Coast in California"},{"id":336006,"rank":11,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372H","text":"Chapter H: General summary of effects of the drought in the Southwest"},{"id":60777,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0372b/plate-1.pdf","text":"Plate 1","size":"3.43 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Areas where annual runoff was less than the median, 1942-57"},{"id":60778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0372b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104445,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4368.htm","size":"7.73 MB","linkFileType":{"id":5,"text":"html"},"description":"4368"},{"id":119888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0372b/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Southwestern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.32226562500001,\n 31.50362930577303\n ],\n [\n -99.49218749999999,\n 31.50362930577303\n ],\n [\n -99.49218749999999,\n 38.95940879245423\n ],\n [\n -120.32226562500001,\n 38.95940879245423\n ],\n [\n -120.32226562500001,\n 31.50362930577303\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0fb6","contributors":{"authors":[{"text":"Gatewood, J. S.","contributorId":100829,"corporation":false,"usgs":true,"family":"Gatewood","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":209190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Alfonso","contributorId":83575,"corporation":false,"usgs":true,"family":"Wilson","given":"Alfonso","email":"","affiliations":[],"preferred":false,"id":209189,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":209187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":209188,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1272,"text":"wsp1757D - 1964 - Ground-water provinces of southern Rhodesia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1757D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1757","chapter":"D","title":"Ground-water provinces of southern Rhodesia","docAbstract":"Ground-water development, utilization, and occurrence in nine ground-water provinces of Southern Rhodesia are summarized in this report. Water obtained from drilled wells for domestic and stock use has played an important part in the social and economic development of Southern Rhodesia from the beginnings of European settlement to the present. Most of the wells obtain water from fractures and weathered zones in crystalline rocks, before recently, there has been an interest in the possibility of obtaining water for irrigation from wells. Studies of the authors indicate that quantities of water sufficient for irrigation can be obtained from alluvial sediments in the S'abi Valley, from Kalahari sands in the western part of the country, are perhaps from aquifers in other areas. \r\n\r\nThe ground-water provinces fall into two groups--those in the crystalline rocks and those in the noncrystalline rocks. Historically, the wells in crystalline rocks, especially the Gold belts province and the Intrusive granites province, have played a major role in supplying water for the needs of man. These provinces, together with two other less important crystalline rock provinces, form the broad arch which constitutes the central core of the country. The noncrystalline rocks overlie and flank the crystalline rocks to the southeast, northwest, and north. The noncrystalline rock provinces, especially the Alluvium-Kalahari province, contain the most productive or potentially productive ground-water reservoirs in Southern Rhodesia and offer promise of supplying water for irrigation and for other purposes.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757D","usgsCitation":"Dennis, P.E., and Hindson, L., 1964, Ground-water provinces of southern Rhodesia: U.S. Geological Survey Water Supply Paper 1757, iii, 15 p. :map ;24 cm. + plate folded in pocket., https://doi.org/10.3133/wsp1757D.","productDescription":"iii, 15 p. :map ;24 cm. + plate folded in pocket.","costCenters":[],"links":[{"id":137504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757d/report-thumb.jpg"},{"id":26226,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2590","contributors":{"authors":[{"text":"Dennis, Philip Eldon","contributorId":8439,"corporation":false,"usgs":true,"family":"Dennis","given":"Philip","email":"","middleInitial":"Eldon","affiliations":[],"preferred":false,"id":143477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hindson, L.L.","contributorId":46924,"corporation":false,"usgs":true,"family":"Hindson","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":143478,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1307,"text":"wsp1779L - 1964 - Discharge ratings for streams at submerged section controls","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1779L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","chapter":"L","title":"Discharge ratings for streams at submerged section controls","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779L","usgsCitation":"Eisenlohr, W.S., 1964, Discharge ratings for streams at submerged section controls: U.S. Geological Survey Water Supply Paper 1779, iii, 32 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1779L.","productDescription":"iii, 32 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779l/report-thumb.jpg"},{"id":26340,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a98a","contributors":{"authors":[{"text":"Eisenlohr, William Stewart","contributorId":36533,"corporation":false,"usgs":true,"family":"Eisenlohr","given":"William","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":143536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68465,"text":"ha200 - 1964 - Chemical quality of public water supplies of the United States and Puerto Rico, 1962","interactions":[],"lastModifiedDate":"2018-02-16T16:16:57","indexId":"ha200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"200","title":"Chemical quality of public water supplies of the United States and Puerto Rico, 1962","docAbstract":"Municipal water systems in the United States and Puerto Rico supply water for many commercial and industrial uses as well as for domestic wells. It is generally known that our water resources are unequally distributed throughout the country, but it is not quite so well understood that the quality of our water resources is also variable. This hydrologic investigations atlas shows, State by State, some of the chemical quality aspects of our public water supplies. This information can be used to evaluate the suitability of the public supplies for many uses – among them, manufacturing processes, food processing, cooling water, and domestic use.
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L.","contributorId":20313,"corporation":false,"usgs":true,"family":"McGuinness","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":629769,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":3226,"text":"cir483 - 1964 - Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"483","title":"Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","docAbstract":"Estimates of potential waterpower and historical data on waterpower developments in various parts of the world are assembled in this report. Salient characteristics of the period studied, 1955-62, include increased use of the underground powerhouse, multiple -purpose developments, and use of storage (including pumped storage) to increase the value of waterpower for peaking purposes. High-voltage long-distance transmission has been improved, especially in the United States, Sweden, and the U.S.S.R., and generating facilities tend to be larger than ever before. Asia leads the continents in total potential waterpower; Europe is first in use of waterpower. In rate of increase of waterpower installations and in percent of hydroelectric to total installations Africa is first among the continents. The 1955-62 period saw a great increase in per capita consumption of electric energy. Norway leads all countries with annual consumption of about 9,000 kwhr per capita. Waterpower development was carried on in a majority of the countries of the world and in most of them at an accelerated rate.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir483","usgsCitation":"Young, L.L., 1964, Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62: U.S. Geological Survey Circular 483, iv, 38 p. ;26cm., https://doi.org/10.3133/cir483.","productDescription":"iv, 38 p. ;26cm.","costCenters":[],"links":[{"id":123048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0483/report-thumb.jpg"},{"id":30219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0483/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6992c4","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146469,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3662,"text":"cir494 - 1964 - Ground water east of Jackson Lake, Grand Teton National Park, Wyoming","interactions":[],"lastModifiedDate":"2022-02-02T21:31:15.484531","indexId":"cir494","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"494","title":"Ground water east of Jackson Lake, Grand Teton National Park, Wyoming","docAbstract":"The project area, which lies east of and adjacent to Jackson Lake is on the downthrown eastern block of the Teton fault, a normal fault that trends northward along the west edge of Jackson Lake. Rocks of pre-Cretaceous age are deeply buried beneath this area. Sedimentary rocks of Cretaceous age and sedimentary and volcanic rocks of Tertiary age, which have an aggregate thickness of about 30,000 feet, are exposed in the northern and eastern parts of the area. Along most of the east side of Jackson Lake, unconsolidated glacial and interglacial deposits of Quaternary age overlie the rocks of Cretaceous and Tertiary age. The unconsolidated deposits were penetrated by test drilling to a depth of 206 feet, but the maximum thickness is probably much greater. Test wells were drilled in five localities to evaluate the deposits of Quaternary age as possible sources of ground water for National Park Service facilities. In the Pilgrim Creek valley, test wells were capable of yielding 200 gpm (gallons per minute); properly constructed production wells could obtain much greater yields. Test wells at Lizard Point and Jackson Lake Campgrounds yielded more than 100 gpm, and a test well near the confluence of the Buffalo Fork and Snake rivers yielded 30 gpm. A test hole drilled in the NW1/4 sec. 36, T. 46 N., R. 115 W., was dry at 200 feet. Unconsolidated deposits of Quaternary age are the most promising source of additional ground water. Because of the extreme range in grain size and sorting, these deposits vary greatly in permeability. Their saturated thickness ranges from 0 to more than 130 feet and changes seasonally; variations of as much as 36 feet were measured (1961-62) in the Pilgrim Creek valley. In most localities where deposits of Quaternary age are ,present, small to moderate ground-water supplies can be developed; larger ground-water supplies can be developed in parts of the Pilgrim Creek valley. One well taps the Bivouac Formation of Late Pliocene or Pleistocene age, but no other wells are known to tap rocks of possible pre-Quaternary age. The Harebell Formation and Bacon Ridge Sandstone of Late Cretaceous age and the Bivouac Formation offer the best possibilities for development of additional water supplies from the consolidated rocks. Chemical analyses of water samples from 11 wells in the deposits of Quaternary age and 1 well in the Bivouac Formation indicate that the water is of generally good quality for drinking and most other purposes. Water from one well tapping lacustrine(?) sand had a dissolved-solids content of 321 ppm (parts per million); all other samples had from 87 to 145 ppm.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir494","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"McGreevy, L., and Gordon, E.D., 1964, Ground water east of Jackson Lake, Grand Teton National Park, Wyoming: U.S. Geological Survey Circular 494, Report: iv, 27 p.; 1 Plate: 16.90 x 21.58 inches, https://doi.org/10.3133/cir494.","productDescription":"Report: iv, 27 p.; 1 Plate: 16.90 x 21.58 inches","numberOfPages":"32","costCenters":[],"links":[{"id":395311,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23905.htm"},{"id":30702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0494/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0494/report-thumb.jpg"},{"id":271081,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0494/plate-1.pdf"}],"country":"United States","state":"Wyoming","otherGeospatial":"Grand Teton National Park, Jackson Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.753173828125,\n 43.8008364060122\n ],\n [\n -110.753173828125,\n 44.067853669357596\n ],\n [\n -110.4345703125,\n 44.067853669357596\n ],\n [\n -110.4345703125,\n 43.8008364060122\n ],\n [\n -110.753173828125,\n 43.8008364060122\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc4f","contributors":{"authors":[{"text":"McGreevy, Laurence J.","contributorId":98706,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence J.","affiliations":[],"preferred":false,"id":147362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, Ellis D.","contributorId":12451,"corporation":false,"usgs":true,"family":"Gordon","given":"Ellis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":147361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6204,"text":"pp469 - 1964 - Cambrian rocks of the Pioche mining district, Nevada: With a section on Pioche shale faunules","interactions":[],"lastModifiedDate":"2022-01-11T19:22:58.368205","indexId":"pp469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"469","title":"Cambrian rocks of the Pioche mining district, Nevada: With a section on Pioche shale faunules","docAbstract":"The Pioche mining district in the Ely Range, southeastern Nevada, is one of several districts in the Great Basin where Cambrian rocks are hosts of important ore deposits. Cambrian strata underlying the Ely Range are intruded by porphyritic granite and other dikes. Tertiary volcanic rocks and Pliocene fresh-water clastic deposits of the Panaca Formation occupy adjacent valleys and extend over the Cambrian strata on the south and east.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp469","usgsCitation":"Merriam, C.W., and Palmer, A.R., 1964, Cambrian rocks of the Pioche mining district, Nevada: With a section on Pioche shale faunules: U.S. Geological Survey Professional Paper 469, Report: iv, 59 p.; 1 Plate: 19.43 × 17.94 inches, https://doi.org/10.3133/pp469.","productDescription":"Report: iv, 59 p.; 1 Plate: 19.43 × 17.94 inches","costCenters":[],"links":[{"id":394196,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4473.htm"},{"id":274603,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0469/plate-1.pdf"},{"id":268957,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0469/report.pdf"},{"id":140077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0469/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Pioche mining district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.75,\n 37.75\n ],\n [\n -114.3333,\n 37.75\n ],\n [\n -114.3333,\n 38.1203\n ],\n [\n -114.75,\n 38.1203\n ],\n [\n -114.75,\n 37.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a04e4b07f02db5f855e","contributors":{"authors":[{"text":"Merriam, Charles Warren","contributorId":14399,"corporation":false,"usgs":true,"family":"Merriam","given":"Charles","email":"","middleInitial":"Warren","affiliations":[],"preferred":false,"id":152295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmer, Allison R.","contributorId":24343,"corporation":false,"usgs":true,"family":"Palmer","given":"Allison","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152296,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}